Yi Luo1, Wenhua Fu2, Bin Wang1, Zhiqing Yuan2, Junliang Sun1,3, Xiaodong Zou1, Weimin Yang2. 1. Department of Materials and Environmental Chemistry, Stockholm University, SE-106 91 Stockholm, Sweden. 2. State Key Laboratory of Green Chemical Engineering and Industrial Catalysis, Sinopec Shanghai Research Institute of Petrochemical Technology, 1658 Pudong Beilu, Shanghai 201208, China. 3. College of Chemistry and Molecular Engineering, Beijing National Laboratory for Molecular Sciences, Peking University, Beijing 100871, China.
Abstract
Zeolites with large cavities that are accessible via wide pore windows are desirable but very rare. They have been dominantly used as catalysts in industry. Here we report a novel porous germanosilicate SCM-25, the zeolite structure containing ordered meso-cavities (29.9 × 7.6 × 6.0 Å3) interconnected by 10- and 12-ring channels. SCM-25 was synthesized as nanosized crystals by using a simple organic structure-directing agent (OSDA). Three-dimensional (3D) electron diffraction shows that SCM-25 crystallizes in the orthorhombic space group Cmmm with a = 14.62 Å, b = 51.82 Å, c = 13.11 Å, which is one of the zeolites with the largest unit cell dimensions. We demonstrate that 3D electron diffraction is a powerful technique for determining the complex structure of SCM-25, including the disorders and distributions of framework atoms silicon and germanium. SCM-25 has a high surface area (510 m2/g) and high thermal stability (700 °C). Furthermore, we propose a potential postsynthetic strategy for the preparation of zeolites with ordered meso-cavities by applying the ADOR (assembly-disassembly-organization-reassembly) approach.
Zeolites with large cavities that are accessible via wide pore windows are desirable but very rare. They have been dominantly used as catalysts in industry. Here we report a novel porous germanosilicate SCM-25, the zeolite structure containing ordered meso-cavities (29.9 × 7.6 × 6.0 Å3) interconnected by 10- and 12-ring channels. SCM-25 was synthesized as nanosized crystals by using a simple organic structure-directing agent (OSDA). Three-dimensional (3D) electron diffraction shows that SCM-25 crystallizes in the orthorhombic space group Cmmm with a = 14.62 Å, b = 51.82 Å, c = 13.11 Å, which is one of the zeolites with the largest unit cell dimensions. We demonstrate that 3D electron diffraction is a powerful technique for determining the complex structure of SCM-25, including the disorders and distributions of framework atoms silicon and germanium. SCM-25 has a high surface area (510 m2/g) and high thermal stability (700 °C). Furthermore, we propose a potential postsynthetic strategy for the preparation of zeolites with ordered meso-cavities by applying the ADOR (assembly-disassembly-organization-reassembly) approach.
Zeolites are technologically
important crystalline microporous
materials that have wide applications in catalysis, adsorption/separation,
and ion-exchange.[1] Their framework structures
are built with TO4 tetrahedra (T= Si, Ge, Al, and B, etc.),
which connect to each other through vertex-sharing of oxygen atoms
in the tetrahedra. Different arrangements and connections of the TO4 tetrahedra can form various crystalline structures with tunable
chemical compositions and uniform pores and/or cavities of molecular
dimensions.[2] The microscopic structure
features of a zeolite, especially the size and shape of pores/cavities
and the dimensionality of channels, significantly govern its macroscopic
properties such as size and shape-selectivity and molecular diffusion
in catalysis and adsorption/separation.[3−5] The search for zeolites
with novel framework topologies and unique pore architectures for
improved catalysis and adsorption/separation has always been the object
of many researches worldwide.To date, the International Zeolite
Association (IZA) has authorized
255 different zeolite framework structures, which can be classified
depending on the ring size of pore openings (defined by the number
of tetrahedra forming the ring), the dimensionality of channel systems,
or the presence of cavities.[6] Pores defined
by 8, 10, and 12 TO4 tetrahedra are considered as small
pores (8-ring), medium pores (10-ring), and large pores (12-ring),
respectively. Among all available zeolites, those with large cavities
have been widely applied in many industrial chemical processes and
dominate the synthetic zeolite market.[6−8] Some examples are LTA (8 × 8 × 8-ring, sphere-like cavity of 10.8
Å in the largest dimension), CHA (8 × 8 ×
8-ring, ellipse-like cavity of 9.9 Å), MWW (10 ×
10-ring, ellipse-like cavity of 19.0 Å), and FAU (12 × 12 × 12-ring, sphere-like cavity of 13.0 Å).
This is because their pore architectures allow both molecular diffusion
and shape-selective catalysis/adsorption.[7−11] Therefore, zeolites with large cavities interconnected
by well-defined pore windows or channels are of great interest.[5,12−15] However, studies on these excellent zeolites have shown that their
maximum capacities in many applications could still be optimized by
increasing the size of pores and/or cavities.[16−18]Significant
efforts have been made to prepare novel zeolites with
unique pore structures, especially those containing extra-large pores
(>12-ring, >8.0 Å).[19−21] Currently, the main strategies
used for preparing zeolites with novel structures are as follows:
(i) predesignation of organic structure-directing agent (OSDA), (ii)
heteroatom substitution, and (iii) topotactic conversion of 2D to
3D, 3D to 3D, and 3D to 2D materials, including the assembly–disassembly–organization–reassembly
(ADOR) approach.[22−24] In the past decades, through the strategy of using
predesigned large, bulky OSDAs and/or heteroatoms, a series of novel
extra-large pore zeolites (EMM-23(*-EWT),[25] ITQ-33(ITT),[26] ITQ-37(-ITV),[27] ITQ-40(-IRY),[28] ITQ-44(IRR),[29] ITQ-51(IFO),[30] and ITQ-43[31] etc.) have been synthesized, some with pores beyond 20 Å, extending
from the microporous range (<20.0 Å) to mesoporous range (20.0–50.0
Å).[1] However, large bulky OSDAs are
often difficult to prepare and are expensive, which hinders the applications
of those extra-large pore zeolites.[22] The
ADOR approach takes advantage of the weakness of the structures of
germanosilicate zeolites to achieve the selective dissolution of germanium
from the structure. It provides the opportunities to prepare novel
zeolite families with continuously controllable porosities that are
unfeasible by traditional solvothermal synthetic methods. However,
so far, the zeolites afforded by ADOR have either irregular mesopores
or micropores with reduced pore sizes compared to the parent zeolite.[24] Alternatively, mesopores can also be introduced
into zeolite crystals via various postsynthetic approaches such as
acid, alkaline, and steam treatments.[32] However, it is challenging to control the size, shape, and location
of mesopores by those treatments. The resulting mesopores are mostly
irregular in terms of sizes and distributions, which may sacrifice
the crystallinity and shape-selectivity of zeolite materials.[11]Zeolites with large cavities that are
accessible via large pore
windows are desirable, because they allow large molecules to enter
the cavities and access the catalytic centers and can also enhance
the shape selectivity and molecular diffusion. While the synthesis
of zeolites with large/meso-cavities connected to small 8-ring pore
windows has been realized in the ABC-6 family,[13,33] there is a lack of strategy to synthesize zeolites with ordered
meso-cavities accessible via medium (10-ring) and large (12-ring)
pore windows. Herein, we report a germanosilicate SCM-25, a zeolite
with a hierarchical pore architecture built of meso-cavities fully
interconnected by medium and large pores. SCM-25 was first synthesized
using a simple and commercially available OSDA in 2019.[34] The structure of SCM-25 was determined from
nanosized crystals by 3D electron diffraction (3D ED),[35−39] more specifically continuous rotation electron diffraction (cRED).[40] The framework of SCM-25 is isostructural to
that of recently reported HMP-16[41] and
closely related to that of ITQ-21,[42] which
has an intersecting 3D 12 × 12 × 12-ring channel system.
A potential postsynthesis strategy for preparing zeolites with meso-cavities
is proposed based on the structural relationship between SCM-25 and
ITQ-21.
Results and Discussion
The germanosilicate zeolite
SCM-25 was synthesized as nanosized
platelike crystals (∼700 × 500 × 30 nm3, Figure S1) in fluoride medium using
1,1,3,5-tetramethyl piperidinium hydroxide (1,1,3,5-TMPOH) as an organic
structure-directing agent (OSDA).[34] It
crystallized from a gel with a molar composition of 0.5 1,1,3,5-TMPOH/0.667
SiO2/0.333 GeO2/0.5 HF/7 H2O at 175
°C for 14 days under dynamic conditions. The detailed descriptions
of the synthesis conditions are given in the Supporting Information.The 13C solid-state MAS NMR of
as-made SCM-25 indicates
that the OSDAs are intact and accommodated in the structure (Figure S2). The Si/Ge molar ratio of the solid
sample is 2.4, as revealed by the inductively coupled plasma-atomic
emission spectrometry (ICP-AES) analysis (Table S1). In situ PXRD shows that SCM-25 has high thermal stability
(>700 °C, Figure S3). Its framework
structure was retained after removing the OSDAs by calcination in
air at 550 °C (Figure S5). The 29Si solid-state MAS and 1H to 29Si CPMAS
NMR spectra of the calcined SCM-25 show that most Si atoms are connected
to four TO4 (Q4 species, Si(OT4), T = Si, Ge, Figure S6).[28,43] The 19F solid-state MAS NMR spectrum implies the existence of double 4-ring
(d4r) units in the structure (Figure S6).[44] N2 adsorption measurements of SCM-25 show a Brunauer–Emmett–Teller
(BET) surface area of 510 m2/g with a micropore volume
of 0.18 cm3/g (Figure S7). Meanwhile,
a bimodal pore size distribution centered at 6.9 and 8.2 Å was
observed (Figure S7).Because of
the nanosize of SCM-25 crystals that are too small for
single-crystal X-ray diffraction, continuous rotation electron diffraction
(cRED) was used for structure determination of SCM-25 (Figures and 2). cRED data were collected on a JEOL JEM2100 transmission electron
microscope (TEM) at 200 kV equipped with a Timepix hybrid pixel detector
using the program Instamatic developed in our lab.[40] A cRED data set with 342 diffraction frames
and rotation range of 90.61° was collected within 3.4 min (Table S2), which shows that SCM-25 has a large C-centered orthorhombic cell of a = 14.62
Å, b = 51.82 Å, c = 13.11
Å, as identified using the program XDS.[45] Based on the reflection conditions observed
from the 3D reciprocal lattice reconstructed from the cRED data by
the program REDp(46) (Figure ), three possible
space groups, Cmmm, Cmm2, and C222, were deduced. Integrated intensities of the reflections
were obtained from the cRED data using XDS with a
high resolution (0.80 Å) and completeness (89.8%) (Table S2). The framework structure of SCM-25
could be solved with the space group Cmmm using the
program SHELXT.[47] All
the 10 framework T atoms and 24 of 26 framework oxygen atoms in the
asymmetric unit were located directly (Figures and S8). While
9 of the 10 T atoms are four-connected, one is three-connected and
disordered at two symmetry-related positions. Two terminal O atoms
coordinated to the disordered T atom could not be located by SHELXT due to the low occupancy (0.5). They were added based
on the geometry of zeolites.[48]
Figure 1
Projections
of the framework structure of as-made SCM-25 (2 ×
1 × 1 unit cells) determined from the cRED data. The occupancies
of Ge atoms were refined, and the locations of F– ions were accurately identified. The half-occupied Si and O atoms
show the disorder. The terminal O atoms are in blue, highlighting
the disorder.
Figure 2
3D reciprocal lattice of as-made SCM-25 reconstructed
from the
cRED data. The reflection conditions deduced from the 3D reciprocal
lattice and the 2D slices of 0kl, h0l, and hk0 are hkl: h + k = 2n,
0kl: k = 2n, h0l: h = 2n, hk0: h + k =
2n, and h00: h =
2n. The possible space groups are Cmmm, Cmm2, or C222.
Projections
of the framework structure of as-made SCM-25 (2 ×
1 × 1 unit cells) determined from the cRED data. The occupancies
of Ge atoms were refined, and the locations of F– ions were accurately identified. The half-occupied Si and O atoms
show the disorder. The terminal O atoms are in blue, highlighting
the disorder.3D reciprocal lattice of as-made SCM-25 reconstructed
from the
cRED data. The reflection conditions deduced from the 3D reciprocal
lattice and the 2D slices of 0kl, h0l, and hk0 are hkl: h + k = 2n,
0kl: k = 2n, h0l: h = 2n, hk0: h + k =
2n, and h00: h =
2n. The possible space groups are Cmmm, Cmm2, or C222.The structural model of SCM-25 was refined against the cRED
data
using the program SHELXLE.[49] The highest possible space group Cmmm was applied
in the refinement, and the more accurate unit cell parameters obtained
from the synchrotron PXRD data were used (Table S3). While all T atoms were refined as mixed Si/Ge sites during
the initial refinement, the refinement showed that Ge atoms were mainly
distributed in the double 4-ring (d4r) units and the other T-sites were then assigned as Si-site. Restraints
on the Si–O bond distances and angles were applied to the disordered
terminal Si and O atoms. All atoms were refined anisotropically, and
the refinement converged to R1 = 0.1848, wR2 = 0.4388, and S = 1.684 for 2283 reflections with F > 2σ(F) and 286 parameters (Figures and S9, Table S3). The occupancies of Ge atoms
and locations
of F– ions could be refined without applying any
restraints. The Si and Ge compositions of three symmetry-independent d4r units were refined to be Si3.4Ge4.6 (d4r#1), Si3.5Ge4.5 (d4r#2),
and Si4.6Ge3.4(d4r#3) (Figure ), which
are highly consistent with the results revealed by the 19F NMR spectrum (Figure S6) and ICP (Table S1). The refined chemical composition is
|F–10|[Si94.7Ge41.3O276] (OSDA and H2O molecules were not included
in the refinement) and is in good agreement with that (|(C9NH20F)10.6(H2O)7.8|[Si96.0Ge40.0O276]) calculated from the
ICP and TGA analysis (Table S1). The bond
lengths are 1.58–1.62 Å (average 1.60 Å) for Si–O
and 1.60–1.69 Å (average 1.65 Å) for Si/Ge–O.
The T–O–T angles range between 103.3° and 114.9°
(average 109.4°), which are chemically reasonable (Table S4). These show the framework structure
determined from cRED data is highly reliable. The high R-values are not due to the inaccurate structural model but most likely
result from dynamical effects due to multiple scattering of electrons
in the crystal and the absence of OSDAs in the model.Rietveld
refinement against the synchrotron powder X-ray diffraction
(PXRD) data of as-made SCM-25 was conducted to locate OSDAs in the
pores (Figure ). The
framework structure determined by cRED was served as a starting model
for Rietveld refinement. During the refinement, the OSDA TMP cations
were treated as rigid bodies and located using the simulated-annealing
algorithm implemented in TOPAS V6.0.[50-52] All framework atoms were refined with soft geometric restraints
of bond distances and angles. The refinement converged with agreement
residuals of RB = 0.033, Rwp = 0.170, with Rexp = 0.099
(Figure and Table S5). The refined chemical composition is
|(C9H20N+)(F–)(H2O)0.93|10[Si96.0Ge40.0O272]. The framework structure refined against the PXRD
data matches very well with the one refined against the cRED data,
with an average deviation in atomic positions by 0.04(2) Å for
the T atoms and 0.10(4) Å for the O atoms (Tables S4 and S6). There are 10 TMP+ cations in
each unit cell, which are distributed at four symmetry-independent
sites (OSDA#a, #b, #c #d) with a partial occupancy of 0.158, 0.148,
0.174, and 0.146, respectively (Figure S10).[50,51] Their positive charges are balanced by the
10 F– ions in the d4r units. These results are consistent with those from NMR, ICP, TGA,
etc. Each TMP+ cation has several possible locations because
of the high symmetry in Cmmm. Electron densities
from the OSDAs could also be identified from the difference electron
density map (Figure S10), which are found
both within and at the pore window of the meso-cavities. Figure S11 illustrates the location of the TMP+ cations in the meso-cavity.
Figure 3
Synchrotron PXRD pattern (blue line, λ
= 0.412836 Å)
of as-made SCM-25 and its Rietveld refinement. The calculated (pink
line) and difference profiles (gray line) of the refinement are also
presented. The profiles in the inset have been magnified by 10 times
to show more details in the high-angle region. The black tick marks
under the profiles are the positions of the Bragg reflections.
Synchrotron PXRD pattern (blue line, λ
= 0.412836 Å)
of as-made SCM-25 and its Rietveld refinement. The calculated (pink
line) and difference profiles (gray line) of the refinement are also
presented. The profiles in the inset have been magnified by 10 times
to show more details in the high-angle region. The black tick marks
under the profiles are the positions of the Bragg reflections.The framework structure of SCM-25 exhibits a novel
topology as
elucidated by the crystallographic programs Topos and 3dt.[53] The three-dimensional
network is composed of nine different tiles (Figure S12). The large complex tile with a face symbol [410·68·108·124] represents
the novel shuttle-like meso-cavity in SCM-25, with a size of 29.9
× 7.6 × 6.0 Å3 (Figures a and S12). The
shuttle-like meso-cavities are accessible via four 12-ring windows
and eight 10-ring windows: two 12-ring (7.6 × 6.8 Å) and
four 10-ring (5.4 × 4.7 Å) windows perpendicular to the c-axis, and two 12-ring (8.0 × 6.1 Å) and four
10-ring (5.6 × 5.1 Å) windows perpendicular to the b-axis (Figure b and Figure S13). This gives rise
to a very open zeolite structure (framework density: 14.7 T/1000 Å3) with a unique 3D 12 × 12 × 10-ring channel system
built of the ordered meso-cavities interconnected by the medium and
large pores. In addition, we found by electron diffraction that the
longest direction of the meso-cavity (along the b-axis) is perpendicular to the nanoplates of SCM-25 crystals (Figure S15). These may be beneficial for diffusion,
adsorption, and reactivity. The meso-cavities in SCM-25 comprise the
unique features of cavities in both FAU (12 × 12
× 12-ring) and MWW (10 × 10-ring) (Figure S14). All these make SCM-25 promising
for catalytic and adsorptive applications.
Figure 4
(a) Nature tile of the
meso-cavity and its locations in the SCM-25
framework. The largest dimension of the meso-cavity is along the b-axis and perpendicular to the crystal. (b) Unique channel
system of SCM-25. The envelope is only meant to show the arrangement
of the channels and meso-cavities within the framework structure.
The image was generated using Material Studio 7.0.[54]
(a) Nature tile of the
meso-cavity and its locations in the SCM-25
framework. The largest dimension of the meso-cavity is along the b-axis and perpendicular to the crystal. (b) Unique channel
system of SCM-25. The envelope is only meant to show the arrangement
of the channels and meso-cavities within the framework structure.
The image was generated using Material Studio 7.0.[54]The framework structure of SCM-25
is closely related to that of
zeolite ITQ-21 (space group Fm–3c, a = 27.698 Å),[42] and both zeolites are built from the same building layer (referred
to as ITQ-21 layer) that contains intersecting 12-ring channels along
three perpendicular directions (Figure ). In ITQ-21, the ITQ-21 layers are connected via d4r units to form a 3D framework with the
straight 12-ring channels along the a-, b-, and c-axes. In SCM-25, the neighboring ITQ-21
layers are shifted by 1/2a (ca. 7.1 Å) from
each other and connected via a tetrahedral pair −O(SiO2)–O–(SiO2)O–(Si2O7). The shift of neighboring ITQ-21 layers blocks the
straight 12-ring channels perpendicular to the layer and turns the
channels into meso-cavities. From the structural point of view, the
framework structure of SCM-25 could be constructed from ITQ-21 via
the ADOR approach,[24] as illustrated in Figure . The assembled ITQ-21
framework is disassembled into ITQ-21 layers by selective removal
of every second d4r unit along the b-axis. The ITQ-21 layers are then reorganized by a shift
(1/2a) along the a-axis (organization)
and connected through tetrahedral pairs (Si2O7) to form the framework structure of SCM-25 (reassembly). We envisage
that the ADOR approach could be used to prepare zeolites with ordered
meso-cavities based on the same principle as shown in Figure . Kasneryk et al. reported
that the unfeasible zeolite IPC-12 could be prepared via the ADOR
approach from the parent zeolite UOV which consists of
porous layers.[55] The d4r units in the UOV framework could
be selectively removed to form layers with tunable thickness by tailoring
their chemical compositions.[56] The layers
can be rearranged with a shift to interrupt the straight channels
and subsequently reassembled by modifying the ADOR conditions.[57] We believe the ADOR approach has also a potential
for synthesizing novel zeolites with ordered meso-cavities by simply
blocking straight channels in a known zeolite.
Figure 5
Structural relationship
between ITQ-21 and SCM-25. The framework
structures of these two zeolites share the same porous layers. The
framework structure of ITQ-21 is possible to be transformed into the
framework structure of SCM-25 via the ADOR approach. This case inspired
us to propose a promising approach to prepare zeolites with meso-cavities
in their framework structures. O atoms have been omitted for clarity.
The corresponding projections viewed along the a-axis
are presented in Figure S16.
Structural relationship
between ITQ-21 and SCM-25. The framework
structures of these two zeolites share the same porous layers. The
framework structure of ITQ-21 is possible to be transformed into the
framework structure of SCM-25 via the ADOR approach. This case inspired
us to propose a promising approach to prepare zeolites with meso-cavities
in their framework structures. O atoms have been omitted for clarity.
The corresponding projections viewed along the a-axis
are presented in Figure S16.It is worth mentioning that SCM-25 is isostructural to that
of
recently reported HPM-16.[41] While SCM-25
was synthesized using a simple and commercially available 1,1,3,5-TMPOH
as the OSDA, the OSDA used for the synthesis of HPM-16, 1-methyl-2-ethyl-3-n-propylimidazolium hydroxide (1M2E3nPrIMOH), is more complex
(Figure ) and requires
several steps to produce.[41] While the 3D
ED data could only provide an initial model of HPM-16 without considering
the distribution of silicon and germanium in the framework, we show
that accurate framework structure of SCM-25 including the locations
of silicon and germanium atoms could be determined. Meanwhile, by
Rietveld refinement against the synchrotron PXRD data, we revealed
four symmetry-independent sites of TMP+ cations in SCM-25,
which is different from the two symmetry-independent sites of 1M2E3nPrIM+ cations in HPM-16. A comparison of the locations of the OSDAs
in the two structures is given in Figure S17. Furthermore, we analyzed the structural relationship between ITQ-21
and SCM-25 and proposed a potential approach to prepare zeolite structures
with ordered meso-cavities.
Figure 6
Molecular structures of 1,1,3,5-TMPOH and 1M2E3nPrIMOH,
used as
the OSDAs for the synthesis of SCM-25 and HPM-16, respectively.
Molecular structures of 1,1,3,5-TMPOH and 1M2E3nPrIMOH,
used as
the OSDAs for the synthesis of SCM-25 and HPM-16, respectively.
Conclusions
In summary, we have
demonstrated the synthesis and structure determination
of a germanosilicate SCM-25, the zeolite containing ordered meso-cavities.
SCM-25 was synthesized using a simple and commercially available OSDA
and is stable after removing the OSDAs by calcination in air. Recent
advances of 3D ED, especially continuous rotation electron diffraction
(cRED), made it possible to determine the complex structure of nanosized
SCM-25 crystals with high reliability. These are also confirmed by
synchrotron PXRD, NMR, ICP, etc. SCM-25 has a unique 3D pore architecture
with meso-cavities accessible via large 12-ring and medium 10-ring
microporous channels. The high thermal stability together with the
unique 3D hierarchical pore architecture makes SCM-25 promising for
catalytic and adsorptive applications. In addition, inspired by the
structural relationship between SCM-25 and zeolite ITQ-21, we proposed
a potential postsynthesis strategy for the preparation of zeolites
with ordered meso-cavities.
Authors: A Corma; M J Díaz-Cabañas; J Jiang; M Afeworki; D L Dorset; S L Soled; K G Strohmaier Journal: Proc Natl Acad Sci U S A Date: 2010-07-26 Impact factor: 11.205
Authors: Jiuxing Jiang; Jose L Jorda; Maria J Diaz-Cabanas; Jihong Yu; Avelino Corma Journal: Angew Chem Int Ed Engl Date: 2010-07-05 Impact factor: 15.336
Authors: Jong Hun Kang; Raimund Walter; Dan Xie; Tracy Davis; Cong-Yan Chen; Mark E Davis; Stacey I Zones Journal: Chemphyschem Date: 2018-01-10 Impact factor: 3.102
Authors: Valeryia Kasneryk; Mariya Shamzhy; Maksym Opanasenko; Paul S Wheatley; Samuel A Morris; Samantha E Russell; Alvaro Mayoral; Michal Trachta; Jiří Čejka; Russell E Morris Journal: Angew Chem Int Ed Engl Date: 2017-03-13 Impact factor: 15.336